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The Linkage Between Methane Fluxes and Gross Primary Productivity at Diurnal and Seasonal Scales on a Rice Paddy Field in Eastern China

涡度相关法 环境科学 大气科学 初级生产 生长季节 水田 温室气体 叶面积指数 日循环 蒸汽压差 大气(单位) 二氧化碳 甲烷 生态系统 农学 生态学 蒸腾作用 气象学 化学 光合作用 地理 生物 生物化学 地质学
作者
Tingting Zhu,Yanlian Zhou,Weimin Ju,J. Li,Lu Hu,Shu Yuan,Xiuli Xing
出处
期刊:Journal Of Geophysical Research: Biogeosciences [Wiley]
卷期号:128 (9) 被引量:1
标识
DOI:10.1029/2023jg007632
摘要

Abstract Carbon dioxide (CO 2 ) and methane (CH 4 ) are the most important two greenhouse gases in the atmosphere which were closely coupled between terrestrial ecosystems and the atmosphere. However, the relationship between CO 2 and CH 4 fluxes of rice paddy at different temporal scales is still unclear. Based on 6 years of eddy covariance measurements on a flooded rice paddy field in Eastern China, the relationship between gross primary productivity (GPP) and CH 4 fluxes and the effects of biophysical and environmental factors on daily CH 4 /GPP were investigated. CH 4 fluxes and GPP were tightly linked at diurnal and seasonal scales. On average, half‐hourly CH 4 fluxes lagged GPP by 1.5 hr while daily GPP lagged CH 4 fluxes by 19 days over the growing season. Leaf area index, water table depth (WTD), air temperature, vapor pressure deficit, and canopy conductance significantly affect daily CH 4 /GPP. A semi‐empirical multiplicative model was able to capture 77% and 84% seasonal variability of daily CH 4 /GPP for the training data set and testing data set, respectively. WTD is a crucial input affecting the performance of the model. Without WTD included, the agreement between estimated and observed daily CH 4 /GPP was weakened. Under the condition without WTD data available, separate calibration of the semi‐empirical multiplicative model before and after panicle initiation could improve the estimation of daily CH 4 /GPP to some extent. The findings in this study enhance our understanding regarding the complex interactions between CH 4 fluxes and GPP in the rice paddy and are helpful for better estimation of CH 4 fluxes from GPP.

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